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Updated: Jan 15, 2026

Synchrotron X-ray Microdiffraction and Fluorescence Imaging of Mineral and Rock Samples
Published on: June 19, 2018
Extending the depth range in energy-dispersive X-ray stress analysis by simultaneous multi-detector data acquisition
Christoph Genzel1, Daniel Apel1, Mirko Boin1
1Department of Microstructure and Residual Stress Analysis Helmholtz-Zentrum Berlin für Materialien und Energie Germany.
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A scattering geometry for depth-resolved energy-dispersive X-ray stress analysis on polycrystalline materials is introduced. Via simultaneous data acquisition during a sin2 ψ measurement using two detectors arranged in the horizontal diffraction plane, it aims to extend the accessible information depth to the free surface as well as deeper material zones. While data acquisition with the first detector takes place in a symmetrical configuration with regard to the incident and exit angles, αi and αe, respectively, the second detector runs in an asymmetrical mode, defined by αi < αe. Therefore, the scattering vectors assigned to the two diffraction geometries run in different tilt planes during a χ scan of the sample performed in the Eulerian cradle. Treatment of the data recorded in the asymmetric diffraction mode requires modifications of the fundamental equation of X-ray stress analysis, which are discussed using the example of measurements performed on a unidirectionally ground ferritic steel sample.

